Paleoseismological implications of liquefaction-induced structures caused by the 2017 Pohang Earthquake
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Paleoseismological implications of liquefaction-induced structures caused by the 2017 Pohang Earthquake' 의 참고문헌
Use of liquefaction-induced features for paleoseismic analysis – an overview of how seismic liquefaction features can be distinguished from other features and how their regional distribution and properties of source sediment can be used to infer the location and strength of Holocene paleo-earthquakes
The earthquake potential of the New Madrid seismic zone
The Latest Fault Movement on the Northern Yangsan Fault Zone around the Yugye-Ri Area, Southeast
The Geology of Fluvial Deposits
Soft sediment deformation structures interpreted as seismites in lacustrine sediments of the Prebetic Zone, SE Spain, and their potential use as indicators of earthquake magnitudes during the Late Miocene
Sedimentary Structures: Their Character and Physical Basis (Vol. II)
Sand blows as a potential tool for magnitude estimation of pre-instrumental earthquakes
Recognising triggers for soft-sediment deformation: current understanding and future directions
Polygenetic sand volcanoes: on the features of liquefaction processes generated by a single event (2012 Emilia Romagna 5.9 Mw earthquake Italy)
New empirical relationships between magnitude and distance for liquefaction
New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement
Miocene tectonic evolution of the basins and fault systems, SE Kora: Dextral, simple shear during the East Sea (Sea of Japan)opening
Minimum earthquake magnitude associated with coseismic surface faulting
Kachchh (Bhuj) earthquake: coseismic surface features and their significance
Identifying triggers for liquefactioninduced soft-sediment deformation in sands
Freshwater megaflood sedimentation: What can we learn about generic processes
Experimental soft-sediment deformation: structures formed by the liquefaction of unconsolidated sands and some ancient examples
Earthquakes in the Southeast Korean Peninsula: focusing on the 2016 Gyeongju and the 2017 Pohang Earthquakes
Determining earthquake recurrence intervals from deformational structures in young lacustrine sediments
Controls and evolution of fan delta systems in the Miocene Pohang basin, SE Korea
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Paleoseismological implications of liquefaction-induced structures caused by the 2017 Pohang Earthquake'
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